Thesis for degree: Licentiate of Engineering
Thesis for degree: Licentiate of Engineering
Thesis for degree: Licentiate of Engineering
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streaming [3]. The concentration ρ ζ is defined similarly as the fluid density in equation (2.7)<br />
[3]:<br />
(2.13)<br />
To avoid numerical instability, it is recommended to keep the relaxation times at the order <strong>of</strong><br />
unity. This would mean that the diffusivity values are adjusted by scaling them up to ensure<br />
relaxation times <strong>of</strong> unity [14-16].<br />
The LB equation can be extended to include several components or species. The equations<br />
remain the same <strong>for</strong> each species but the interaction and combination <strong>of</strong> the streaming and<br />
collision action <strong>for</strong> species i is defined as [3, 14-16].<br />
(2.14)<br />
where f i a is the PDF, e i a the velocity and<br />
time t along the direction a <strong>for</strong> species i.<br />
a i the collision term at any spatial location x and<br />
Streaming is described in two steps. The PDFs, <strong>for</strong> example <strong>for</strong> species 1, are streamed from<br />
one lattice point to the adjacent lattice points, while PDFs <strong>for</strong> the remaining species, i.e.,<br />
species 2 and 3, are streamed from one lattice point to <strong>of</strong>f-lattice points in the first step. Offlattice<br />
points are defined as sites which are not related to the current start point. In the second<br />
step, the PDF values <strong>for</strong> species 2 and 3 are determined by interpolation at lattice points. The<br />
collision concept is divided into self-collision, i.e., collision between particles <strong>of</strong> the same<br />
species and cross-collision, i.e., collision between particles <strong>of</strong> different species when the<br />
relative velocity between particles <strong>of</strong> the different species is non-zero [14-16].<br />
For the porous media, the collision term is considered as a second intermediate step after the<br />
streaming [3]. Finally if there are multiple species, the LB model is adjusted by upgrading the<br />
distribution function by also including a composite velocity:<br />
(2.15)<br />
where τ is the relaxation time and i represents the different components involved [3].<br />
To <strong>for</strong>m a realistic model, it is possible to include an external <strong>for</strong>ce, e.g., gravitational <strong>for</strong>ce,<br />
on the particles or interaction <strong>for</strong>ces between the particles. This <strong>for</strong>ce is incorporated in a<br />
velocity term which is added to the velocity calculation. These parts are defined as [3]:<br />
(2.16)<br />
(2.17)<br />
where F is the <strong>for</strong>ce acting on the particle, m the mass and a the acceleration <strong>of</strong> the particle.<br />
Further, u is the velocity, ρ the density and τ the relaxation time.<br />
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